| Location |
| NAD 83 |
50° 52' 00.00'' N, 120° 34' 05.00'' W
50.866667, -120.568056
UTM: Easting 671127, Northing 5637816, Zone 10 (North)
|
| NAD 27 |
50° 52' 00.22'' N, 120° 34' 01.04'' W
50.866727, -120.566956
UTM: Easting 671210, Northing 5637606, Zone 10 (North)
|
| NTS |
092I15E |
| BCGS |
092I088 |
|
| Geological Summary |
MIOCENE AGE PLATEAU BASALT IS LOCALLY ERODED TO EXPOSE A MIXED ASSEMBLAGE OF ANDESITE TUFFS, CARBONATED GREENSTONE, PERIDOTITE? AND GABBRO, WHICH ARE INTRUDED BY SEVERAL NORTHEAST STRIKING FELDSPAR PORPHYRY DYKES. LOW-GRADE GOLD-PYRITE MINERALIZATION IS ASSOCIATED WITH QUARTZ VEINING AND STOCKWORK IN OR ADJACENT TO THE FELDSPAR PORPHYRY DYKES. RESULTS OF OLD WORKINGS HAVE FAILED TO SUBSTANTIATE PREVIOUSLY REPORTED HIGH GOLD ASSAYS.
|
